On the Consistent Scaling of Terms in the Sea-Ice Dynamics Equation

W. M. CONNOLLEY; J. M. GREGORY; E. HUNKE; A. J. MCLAREN

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On the Consistent Scaling of Terms in the Sea-Ice Dynamics Equation

机译：关于海冰动力学方程项的一致标度

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The standard way in which the sea-ice dynamics equation is used in models assumes that the wind stress and ocean drag do not depend on the sea-ice concentration. It is demonstrated that this assumption is inconsistent with the free-drift limit, and how great an effect it has in practice is examined. By examining the momentum balance in the free-drift limit, the authors determine the proper area scaling for the forcing terms, thereby obtaining a more accurate solution, particularly in low-ice-concentration regions.

机译：在模型中使用海冰动力学方程式的标准方法是假定风应力和海洋阻力不取决于海冰浓度。事实证明，该假设与自由漂移极限不一致，并且在实践中检验了其影响有多大。通过检查自由漂移极限中的动量平衡，作者确定了强迫项的适当面积比例，从而获得了更准确的解决方案，尤其是在低冰浓度地区。

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来源
《Journal of Physical Oceanography》 |2004年第7期|p.1776-1780|共5页
作者
W. M. CONNOLLEY; J. M. GREGORY; E. HUNKE; A. J. MCLAREN;
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作者单位

British Antarctic Survey, High Cross, Cambridge CB3 0ET, United Kingdom;

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正文语种 eng
中图分类海洋学;
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On the Consistent Scaling of Terms in the Sea-Ice Dynamics Equation

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